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The AAPG/Datapages Combined Publications Database
AAPG Special Volumes
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The Florence field occupies a strip 3 miles wide on the eastern limb of a geosyncline. The oil occurs in fissures in the Pierre shale. The general dip throughout the field ranges from 2° to 5° westward. The eastern boundary of the field is a steep monocline that brings the productive beds to the surface. The western boundary coincides approximately with the occurrence of a heavy sandstone overlying the Pierre shale. Possibly the removal of the sandstone allowed the fissures to open and the oil to accumulate. Thus the accumulation may be as recent as present topography.
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